Respuesta :
A Final statement or concluding statement
Answer:
Rising parcels of unsaturated (clear) air cool at a Faster rate than rising parcels of saturated (cloudy) air.
What will increase in a rising parcel of unsaturated air?
Changes in the local atmospheric pressure occur when air moves vertically in the atmosphere. These pressure variations lead a sinking parcel to be compressed as surrounding pressures rise, and a rising parcel to expand as surrounding pressures fall.
Unsaturated rising air cools and expands at a rate of 9.8 C per 1000 m.
Unsaturated air that is sinking heats and compresses at the same pace.
Unsaturated air rising in the atmosphere expands, cools, and may eventually become saturated.
Ascent will resume after saturation to keep the expansional cooling going. However, moisture will cause some heating to occur inside the package.
When water vapour condenses into droplets or deposits as ice crystals, latent heat is transferred to the air in the parcel, causing this warming to happen.
To learn more about Saturated and Unsaturated air from the given link
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